瘤背石磺体腔细胞分类、免疫相关酶特性及初步转录组学分析

瘤背石磺(Onchidium struma)广泛分布于潮间带和潮下带,是海洋生物向陆地生物辐射进化的重要代表,也是环境监测的指示生物.为丰富瘤背石磺的基础免疫学资料,本文研究了瘤背石磺体腔细胞的类别、细胞密度和体腔液免疫相关酶活性,并通过RNA-Seq测序获得体腔细胞转录本,进行生物信息学分析.结果表明,瘤背石磺主要有...     

瘤背石磺体内重金属铜和镉的净化研究

为降低瘤背石磺(Onchidium struma)体内超标重金属铜和镉的含量,保证其食品安全,作者通过底泥添加木鱼石土(富含锌、硒等)、饲料添加蛋白核小球藻(Chlorella pyrenoidosa)粉以及维生素C对瘤背石磺体内Cd和Cu进行净化,探究不同实验组对瘤背石磺体内Cd和Cu的净化效果。结果表明,对照组单纯用玉米粉暂养对瘤背石磺重金属的排出有一定的效果,但远远低于试验组在底泥中添加木鱼石土、在饲料中添加蛋白核小球藻粉及维生素C的效果。在瘤背石磺产品生产过程中,通过在底泥中添加木鱼石土、在饲料中添加蛋白核小球藻粉及维生素C能高效地降低其体内重金属铜和镉的含量,达到可食用的目的,保证食品安全。     

盐度对瘤背石磺幼贝存活、生长性能和肌肉生化成分的影响

为探讨盐度对瘤背石磺(Onchidium struma)幼贝生长和肌肉生化成分的影响,用不同盐度水平(5、15、25、35和45)的人工海水饲养瘤背石磺幼贝[干质量(2.96±1.02)g]60 d后测定瘤背石磺生长性能和肌肉营养成分。结果显示:(1)瘤背石磺在盐度25~45时生长良好,成活率在90%以上。同时,在盐度25时增重率、特定生长率和蛋白质效率均显著高于其余各盐度组(P0.05),而饲料系数也显著降低(P0.05)。(2)随着盐度的升高,瘤背石磺肌肉水分显著降低(P0.05),粗灰分呈先下降后上升趋势,但对肌肉钙和磷含量影响差异不显著(P0.05);粗蛋白含量在盐度25时最高,为76.66%,而粗脂肪在高盐度时呈显著上升趋势(P0.05),分别在盐度25和45时含量最低和最高。(3)除了谷氨酸、天门冬氨酸和脯氨酸等呈味氨基酸受盐度影响差异显著外,大多数氨基酸均随着盐度升高呈现先上升后下降的趋势,且在盐度25最高,但差异不显著。(4)盐度对于每一种脂肪酸的影响均差异显著,在盐度5至35范围内,n-3 PUFA和n-6 PUFA均呈现上升趋势,但n-3 PUFA/n-6 PUFA值也逐渐升高。与大多数海水贝类不同的是,瘤背石磺DHA含量远低于EPA。试验结果表明,盐度对瘤背石磺生长性能以及肌肉生化成分有显著影响,适宜的盐度可改善瘤背石磺的肌肉品质和风味。     

4种石磺科贝类的胆甾醇含量测定

将瘤背石磺(Onchidium struma)、里氏拟石磺(Paraoncidium reevesii)、平疣桑椹石磺(Platevindex mortoni)和紫色疣石磺(Peronia verruculata)样品,经活体解剖取四种石磺肌肉组织,运用高效液相色谱法对其可食部分进行了胆甾醇含量测定。结果表明:瘤背石磺胆甾醇平均浓度最高,达5 870.00 mg/kg;平疣桑椹石磺、紫色疣石磺、里氏拟石磺的胆甾醇平均质量分别为3 480.00、388.00、316.00 mg/kg,统计分析显示四种石磺可食部分的胆甾醇含量差异显著。     

瘤背石磺营养成分分析及品质评价

利用常规营养测定方法测定了10只瘤背石磺（Onchidium struma）的营养成分。结果表明,瘤背石磺活体（鲜样）的水分、粗灰分、粗蛋白、粗脂肪质量分数分别为88．78％、3．95％、6．30％和0．63％。其肌肉中含17种氨基酸,总质量分数为55．77％（脱脂干样）,其中,7种人体必需氨基酸总含量为15．63％,占氨基酸总量的27．80％。瘤背石磺必需氨基酸比例符合联合国棉农组织／世界卫生组织标准。瘤背石磺的限制性氨基酸是赖氨酸和色氨酸,4种鲜味氨基酸干样的总质量分数为25．33％。瘤背石磺不同部位的蛋白含量不同,表现为精卵巢蛋白〉腹足蛋白〉外套蛋白〉肝脏蛋白,且差异显著（P〈0．05）。矿物质元素含量丰富,钙、磷、铁、锌、铜含量较多,比例适宜,脂溶性维生素A、D、E含量丰富。营养成分分析结果表明,瘤背石磺具有较高的食用价值和保健作用。     

海南岛3种石磺肌肉组织营养成分分析

参照国家食品营养成分分析相关标准,结合液相色谱仪,元素分析仪,电感耦合等离子光谱仪等测定海南岛采集的瘤背石磺(Onchidium struma),紫色疣石磺(Peronia verruculata),平疣桑葚石磺(Platevindex mortoni)3种石磺肌肉组织中营养成分。结果表明:海南岛3种石磺均属于高蛋白质低脂肪的海产品,蛋白质含量达65.0%以上,其中以平疣桑葚石磺蛋白质含量最高;瘤背石磺肌肉组织多糖含量高达30.96%±1.48%,显著高于其他2种石磺;3种石磺肌肉组织中氨基酸组成全面,且以呈味氨基酸含量最高,均达5.60%以上;3种石磺肌肉组织均含有丰富的矿质元素,其中以钙和镁元素含量最高,含量达20~30 g/kg,同时钠和钾元素含量达3.0~6.5 g/kg。海南岛3种石磺均具有丰富的营养价值,其中以高蛋白高多糖低脂肪的瘤背石磺最具有开发前景。     

不同规格瘤背石磺(Onchidium struma)肌肉的生化组成及营养价值评价

提要采用生化测定方法对不同规格瘤背石磺的肌肉指数、肌肉中常规生化成分、氨基酸组成、脂类和脂肪酸组成进行了系统的研究。结果表明:(1)随着体重的增加,瘤背石磺的肌肉指数和肌肉的蛋白质含量均呈下降趋势,而脂肪和碳水化合物含量呈上升趋势,大规格组瘤背石磺肌肉中的蛋白质、脂肪和碳水化合物含量分别为55.20%、9.10%和17.38%。(2)随着体重的增加,肌肉中的氨基酸总量呈显著下降趋势。成体瘤背石磺肌肉中检测出17种氨基酸,其中含有9种人体必需氨基酸,天冬氨酸和谷氨酸为瘤背石磺肌肉中的主要鲜味氨基酸,除蛋氨酸+胱氨酸和色氨酸外,其余必需氨基酸含量均符合FAO/WHO/UNU(1985)的理想模式。(3)不同规格组瘤背石磺肌肉中的脂类和脂肪酸组成接近,肌肉中磷脂含量达80%以上,肌肉中的脂肪酸组成平衡(S∶M∶P接近于1∶1∶1),成体n3-PUFA/n6-PUFA值为1.0左右,而∑PUFA和∑HUFA分别达30.53%和21.78%。     

不同孵化方式、培育密度和附着基对瘤背石磺人工繁育的影响

为提高瘤背石磺(Onchidium struma)在胚胎发育和幼虫发育过程中受精卵的孵化速率和幼虫的存活率, 本试验模拟滩涂生态环境对瘤背石磺亲贝进行人工养殖, 并促使其交配产卵。将采集的瘤背石磺新鲜卵块置于盐度18, 水温25～26 ℃的水体中进行孵化。比较3 种不同孵化方式对孵化速率的影响, 并研究不同孔径(1.0～1.5 mm)海绵附着基和不同培育密度对幼虫存活率的影响, 同时结合幼虫在各水层中分布的变化规律, 探索瘤背石磺胚胎发育和幼虫发育过程的关键技术。结果显示, 采用3 种方式(“喷淋”、“露空”和“梯笼”)孵化, 受精卵至出膜面盘幼虫期所需时间分别为8、6 和9 d; 大孔径(1.2～1.5 mm)海绵组对幼虫的附着效果较好, 存活率显著高于小孔径(1.0～1.2 mm)海绵组(P<0.05),且两者均显著高于未添加附着基组(P<0.05); 存活率与不同培育密度的二次多项式回归分析显示, 瘤背石磺幼虫培育密度为55～61 个/mL 时存活率较高。上述结果表明, “露空”孵化方式能显著缩短瘤背石磺孵化所需时间; 在生产过程中, 幼虫培育密度以55～61 个/mL 为宜, 面盘幼虫期投放大孔径海绵作为幼虫附着基能显著提高幼虫存活率且能明显缩短胚胎发育和幼虫发育所需时间。     

Mian状黄姑鱼早期发育阶段的摄食与生长特性

１９９７年４－５月,在集美大学水产学院海水育苗试验场。采用生态学方法对人工培育的Ｍｉａｎ状黄姑鱼仔、稚、幼鱼的摄食和生长特性进行分析。结果表明,在人工培育条件下,仔、稚、幼鱼的摄食率达９７．９％,摄食量占体重的１．４－２３．４％,日摄食量占体重的３６．４７－６５．１９％;摄食具明显的昼夜节律,黄昏和早晨为摄食高峰;对较大个体的饵料生物有明显的选择性;饵料密度对摄食量有一定影响。摄食量与体重的关系式     

点带石斑鱼人工育苗技术

通过58批次的人工育苗试验，总结点带石斑鱼人工育苗技术；阐述了育苗池、育苗的环境条件、鱼苗不同生长阶段的饵料及投喂方法、育苗水质管理及生产中的操作方法等；讨论了如何解决开口饵料问题和出现3个危险期的原因等。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.